Short-Period
Short-Period : In traditional seismometry with limited dynamic range, seismographs were naturally divided into two types; longperiod seismographs for periods above the spectral peak (periods around 5 seconds) of the microseismic noise generated by ocean waves and short-period seismographs for periods below it. A short-period seismograph response usually has a bandwidth from about 1 to 10 Hz. See Fig. 3.11 ??? in Chapter 3, Section 4.2 in Chapter 4 of this Manual, and Wielandt (2002)
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